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In recent years, continuous radio-noise recording is in use at many geophysical observatories, in order to detect possible earthquake precursors and/or coseismic signals. The recordings obtained indicate that electromagnetic radiation (e.g., in the range of 10-40 kH) can indeed be treated as seismic precursor. We present here the examples of successful prediction observation, which we have obtained in the Central Apennines region at the l'Aquila Observatory (Polish-Italian cooperation). A short discussion on relation between the evolution of stresses (dislocation dynamics) and electromagnetic emission supplements this paper.
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Tom
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43--53
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Bibliogr. 24 poz.
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- Institute of Geophysics, Polish Academy of Sciences, Warszawa, Poland, RT@igf.edu.pl
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Bibliografia
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bwmeta1.element.baztech-article-BSL8-0002-0038